Articles | Volume 9, issue 3
https://doi.org/10.5194/os-9-561-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-9-561-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
14 Jun 2013
Research article |
| 14 Jun 2013
Exceptional dense water formation on the Adriatic shelf in the winter of 2012
H. Mihanović
Hydrographic Institute of the Republic of Croatia, Split, Croatia
I. Vilibić
Institute of Oceanography and Fisheries, Split, Croatia
S. Carniel
CNR – Istituto di Scienze Marine, Venice, Italy
Meteorological and Hydrological Service of Croatia, Zagreb, Croatia
DISVA, Università Politecnica delle Marche, Ancona, Italy
CNR – Istituto di Scienze Marine, Bologna, Italy
A. Bergamasco
CNR – Istituto di Scienze Marine, Venice, Italy
N. Bubić
Institute of Oceanography and Fisheries, Split, Croatia
Z. Ljubešić
Division of Biology, Faculty of Science, University of Zagreb, Zagreb, Croatia
D. Viličić
Division of Biology, Faculty of Science, University of Zagreb, Zagreb, Croatia
A. Boldrin
CNR – Istituto di Scienze Marine, Venice, Italy
V. Malačič
National Institute of Biology, Marine Biological Station, Piran, Slovenia
M. Celio
Regional Environmental Protection Agency – ARPA FVG, Palmanova, Italy
C. Comici
Istituto Nazionale di Oceanografia e di Geofisica Sperimentale – OGS, Trieste, Italy
F. Raicich
CNR – Istituto di Scienze Marine, Trieste, Italy
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The hydrography and circulation west of Sardinia, observed in June 2014 during REP14-MED by means of various measuring platforms, are presented and compared with previous knowledge. So far, the circulation of this area is not well-known and the hydrography is subject to long-term changes. The different water masses are characterized and temporal changes are emphasized. The observed eddies are specified and geostrophic transports in the upper ocean are presented.
Sandro Carniel, Judith Wolf, Vittorio E. Brando, and Lakshmi H. Kantha
Ocean Sci., 13, 495–501, https://doi.org/10.5194/os-13-495-2017, https://doi.org/10.5194/os-13-495-2017, 2017
Branka Ivančan-Picek, Martina Tudor, Kristian Horvath, Antonio Stanešić, and Stjepan Ivatek-Šahdan
Nat. Hazards Earth Syst. Sci., 16, 2657–2682, https://doi.org/10.5194/nhess-16-2657-2016, https://doi.org/10.5194/nhess-16-2657-2016, 2016
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In this paper an overview of the IOPs that affected the Adriatic area during SOP1 HyMeX campaign is presented. Results in this paper highlight the need for an intensive observation period in the future over the Adriatic region. The aim is to better understand the relevant processes and validate the simulated mechanisms as well as to improve numerical forecasts via data assimilation and improvements of model representation of moist processes and sea–land–atmosphere interactions.
Paolo Oddo, Andrea Storto, Srdjan Dobricic, Aniello Russo, Craig Lewis, Reiner Onken, and Emanuel Coelho
Ocean Sci., 12, 1137–1153, https://doi.org/10.5194/os-12-1137-2016, https://doi.org/10.5194/os-12-1137-2016, 2016
Renata Archetti, Agnese Paci, Sandro Carniel, and Davide Bonaldo
Nat. Hazards Earth Syst. Sci., 16, 1107–1122, https://doi.org/10.5194/nhess-16-1107-2016, https://doi.org/10.5194/nhess-16-1107-2016, 2016
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An application to monitor the response of a beach to single storms, in order to predict shoreline changes and to plan the defence of the shore zone is presented. On the study area, Jesolo (Italy), video and current stations were installed. The methodology, which is economically attractive, proves to be a valuable system for providing detailed indications on beach erosion processes and can be used for improving the collaboration between coastal scientists and managers to solve beach-maintenance problems.
Francesco Marcello Falcieri, Lakshmi Kantha, Alvise Benetazzo, Andrea Bergamasco, Davide Bonaldo, Francesco Barbariol, Vlado Malačič, Mauro Sclavo, and Sandro Carniel
Ocean Sci., 12, 433–449, https://doi.org/10.5194/os-12-433-2016, https://doi.org/10.5194/os-12-433-2016, 2016
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Between January 30th and February 4th we collected the first turbulence observations in the Gulf of Trieste under different wind forcing and water column structure. The vertical profiles of the turbulence kinetic energy dissipation rates showed that the presence near the sea floor of different water masses, inflowing from the open sea, can prevent the complete mixing of the water column. This dumping effect is enhanced when these masses present higher suspended sediment concentrations.
Francesco Barbariol, Francesco Marcello Falcieri, Carlotta Scotton, Alvise Benetazzo, Sandro Carniel, and Mauro Sclavo
Ocean Sci., 12, 403–415, https://doi.org/10.5194/os-12-403-2016, https://doi.org/10.5194/os-12-403-2016, 2016
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The analysis presented in the paper aims at extending the classification capabilities of Self-Organizing Maps (SOM) within the context of ocean waves. Indeed, the intrinsic SOM difficulty in representing extremes of the wave climate is discussed and alternative strategies are proposed in order to represent the whole wave climate at a given location. Among them, a two-step SOM together with a double-side map provides the best results.
V. E. Brando, F. Braga, L. Zaggia, C. Giardino, M. Bresciani, E. Matta, D. Bellafiore, C. Ferrarin, F. Maicu, A. Benetazzo, D. Bonaldo, F. M. Falcieri, A. Coluccelli, A. Russo, and S. Carniel
Ocean Sci., 11, 909–920, https://doi.org/10.5194/os-11-909-2015, https://doi.org/10.5194/os-11-909-2015, 2015
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Sea surface temperature and turbidity, derived from satellite imagery, were used to characterize river plumes in the northern Adriatic Sea during a significant flood event in November 2014. Circulation patterns and sea surface salinity, from an operational coupled ocean-wave model, supported the interpretation of the plumes' interaction with the receiving waters and among them.
M. Tudor
Geosci. Model Dev., 8, 2627–2643, https://doi.org/10.5194/gmd-8-2627-2015, https://doi.org/10.5194/gmd-8-2627-2015, 2015
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Limited area models (LAMs) require lateral boundary conditions that are usually available with an interval of several hours. Consequently, LAMs can miss a rapidly moving item that enters the LAM domain. Here we present how to detect a rapidly moving pressure disturbance in fields provided in the coupling files.
F. Raicich
Nat. Hazards Earth Syst. Sci., 15, 527–535, https://doi.org/10.5194/nhess-15-527-2015, https://doi.org/10.5194/nhess-15-527-2015, 2015
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Daily sea level data of the Venice Lagoon observed in the 18th century allow us to obtain a composite the time series of sea level anomalies relative to the mean sea level, spanning 1751--1769 and 1872--2004. From these data the frequency of remarkable storm surges is estimated. They appear to be more frequent in the second half of the 18th century than in the late 19th and 20th centuries. The historical flood on 4 November 1966 turns out to be the most severe during the entire period.
M. Tudor and I. Janeković
Ocean Sci. Discuss., https://doi.org/10.5194/osd-11-2939-2014, https://doi.org/10.5194/osd-11-2939-2014, 2014
Revised manuscript not accepted
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The south-eastern parts of the Adriatic Sea coastline were severely polluted by large amounts of accumulated waste material in the second half of November 2010. In the study we analysed meteorological and oceanographic conditions that lead to the waste deposition using available in situ measurements, remote sensing data as well numerical models of the ocean and the atmosphere.
P. Malanotte-Rizzoli, V. Artale, G. L. Borzelli-Eusebi, S. Brenner, A. Crise, M. Gacic, N. Kress, S. Marullo, M. Ribera d'Alcalà, S. Sofianos, T. Tanhua, A. Theocharis, M. Alvarez, Y. Ashkenazy, A. Bergamasco, V. Cardin, S. Carniel, G. Civitarese, F. D'Ortenzio, J. Font, E. Garcia-Ladona, J. M. Garcia-Lafuente, A. Gogou, M. Gregoire, D. Hainbucher, H. Kontoyannis, V. Kovacevic, E. Kraskapoulou, G. Kroskos, A. Incarbona, M. G. Mazzocchi, M. Orlic, E. Ozsoy, A. Pascual, P.-M. Poulain, W. Roether, A. Rubino, K. Schroeder, J. Siokou-Frangou, E. Souvermezoglou, M. Sprovieri, J. Tintoré, and G. Triantafyllou
Ocean Sci., 10, 281–322, https://doi.org/10.5194/os-10-281-2014, https://doi.org/10.5194/os-10-281-2014, 2014
M. Tudor
Geosci. Model Dev., 6, 901–913, https://doi.org/10.5194/gmd-6-901-2013, https://doi.org/10.5194/gmd-6-901-2013, 2013
S. Pasquet, I. Vilibić, and J. Šepić
Nat. Hazards Earth Syst. Sci., 13, 473–482, https://doi.org/10.5194/nhess-13-473-2013, https://doi.org/10.5194/nhess-13-473-2013, 2013
Related subject area
Approach: In situ Observations | Depth range: Shelf-sea depth | Geographical range: Mediterranean Sea | Phenomena: Temperature, Salinity and Density Fields
Present climate trends and variability in thermohaline properties of the northern Adriatic shelf
Factors favouring phytoplankton blooms in the northern Adriatic: towards the northern Adriatic empirical ecological model
Ivica Vilibić, Petra Zemunik, Jadranka Šepić, Natalija Dunić, Oussama Marzouk, Hrvoje Mihanović, Clea Denamiel, Robert Precali, and Tamara Djakovac
Ocean Sci., 15, 1351–1362, https://doi.org/10.5194/os-15-1351-2019, https://doi.org/10.5194/os-15-1351-2019, 2019
R. Kraus, N. Supić, and R. Precali
Ocean Sci., 12, 19–37, https://doi.org/10.5194/os-12-19-2016, https://doi.org/10.5194/os-12-19-2016, 2016
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Seasonal and interannual production changes in the northern Adriatic (NA) reflect on the total Adriatic bioproduction of certain species (i.e. anchovy). Long-term (1990-2004) phyto-abundance and geostrophic current analysis relieve the basic mechanism of NA biomass production changes. The results present a first step in building an empirical ecological model of the region, aiming to predict the amount of organic production in NA, which is to be used in the environmental management of the region.
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